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Numerical modeling of tide-surge interaction along Orissa coast of India

机译:印度奥里萨邦海岸潮浪相互作用的数值模拟

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摘要

The Orissa coast of India is one of the most vulnerable regions of extreme sea levels associated with severe tropical cyclones. There was extensive loss of life and property due to the October 1999 super cyclone, which devastated large part of the Orissa coast The shallow nature of the head bay, presence of a large number of deltas formed by major rivers of Orissa such as Mahanadi and Dhamra, and high tidal range are responsible for storm surge flooding in the region. Specifically, rising and fallingtidal phases influence the height duration, and arrival time of peak surge along the coast. The objective of the present study is to evaluate the tide-surge interaction during the 1999 Orissa cyclone by using nonlinear vertically integrated numerical models. The pure tidal solution for the head bay region of the Bay of Bengal provides the initial condition for the fine resolution nested grid Orissa model. However, the feedback from the Orissa model does not affect the head bay model as the study provides a one-way interaction. Numerical experiments are performed to study the tide-surge interaction by considering various relative phases of the tidal waves with the surge-wave produced by 1999 Orissa cyclone. The comparison, although utilizing only thelimited estimates of tidal data, appears adequate to assert that the principal features are reproduced correctly.
机译:印度的奥里萨邦海岸是与严重热带气旋有关的极端海平面最脆弱的地区之一。由于1999年10月的超级旋风摧毁了奥里萨邦的大部分地区,造成了生命和财产的广泛损失。头湾的浅层性质,由奥里萨邦主要河流如马哈纳迪河和达姆拉河形成的大量三角洲的存在,以及较高的潮汐范围是造成该地区风暴潮泛滥的原因。具体来说,潮汐的上升和下降阶段会影响高度持续时间以及沿海岸峰潮的到达时间。本研究的目的是通过使用非线性垂直积分数值模型来评估1999年奥里萨邦旋风中的潮-潮相互作用。孟加拉湾头湾区域的纯潮汐解决方案为高分辨率嵌套网格奥里萨邦模型提供了初始条件。但是,由于研究提供了一种单向交互作用,因此来自Orissa模型的反馈不会影响头枕模型。通过考虑潮汐波与1999年Orissa气旋产生的浪涌的各种相对相位,进行了数值实验来研究潮汐-浪涌相互作用。尽管仅利用了潮汐数据的有限估计,但比较似乎足以断言主要特征已正确再现。

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